Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Neoproterozoic


Information provided by geoscience team at Ahmadu Bello University, Zaria, Nigeria --see About

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Zurak Formation
Click to display on map of the Ancient World at:
Zurak Fm base reconstruction

Zurak Fm


Period: 
Cretaceous

Age Interval: 
Cenomanian-Turonian


Province: 
Benue Trough Central

Type Locality and Naming

Not yet given.

References: Reyment, 1965; Adeleye, 1975; Kogbe, 1976; Dessauvagie, 1975; Petters, 1978; Offodile, 1980; Whiteman, 1982; Benkhelil, 1989; Okosun, 1992; Guiraud, 1993; Akande et al., 1998; Zaborski et al., 1998; Jauro et al., 2007; Obaje, 2009; Nwajide, 2013


Lithology and Thickness

Zurak Fm: It is made up of fine to medium, moderately well sorted feldspathic sandstone within thin shales. Thickness is not for certain known.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

Overlies the Keana Fm

Upper contact

Underlies the Makurdi Fm

Regional extent

Benue Trough Central . Equivalent of the Yolde Fm and Pindiga Fm in the Upper Benue Trough.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[8.4,8.5],[8.6,7.1],[8.9,7.2],[8.7,7.5],[9.4,7.5],[11.1,8.8],[10.7,9.2],[8.4,8.5]]]]}}

Fossils

Ammonites (Euomphaloceras septemseriatum, Hoplitoides ingens), Foraminifera, bivalves (Costagyraolis iponensis), Gastropods


Age 

Middle Cretaceous. The four formations indicated in the Cenomanian through mid-Turonian interval are given quasi-equal durations here (Keana Fm = Early Cenomanian, Zurak Fm = Middle Cenomanian, Makurdi Fm = Late Cenomanian, and the Wukari Fm = lower Turonian)

Age Span: 

    Beginning stage: 
Cenomanian

    Fraction up in beginning stage: 
0.3

    Beginning date (Ma): 
98.52

    Ending stage: 
Cenomanian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
95.88

Depositional setting

Marine depositional environment, specifically a shallow to moderately deep marine setting. The presence of organic-rich shales suggests periods of low oxygen levels, likely associated with restricted circulation or high productivity.


Depositional pattern:  


Additional Information


Compiler:  

Enam O. Obiosio, Solomon Joshua Avong and Henry Nasir Suleiman (2024)- Stratigraphic Lexicon compiled from the following books:

Nigeria: Its Petroleum Geology, Resources and Potential, by Arthur Whiteman, 1982; (Volume 1) Published by Graham and Trotman Ltd.

A review of the Cretaceous System in Nigeria by P. M. Zaborski (1998) In Africa Geoscience Review, Vol.5, No.4, pp385-483

Geology and Mineral Resources of Nigeria by Nuhu George Obaje, Published by Springer-Verlag Berlin Heidelberg 2009; http://www.springer.com/series/772

Geology of Nigeria Sedimentary Basins, Nwajide C. S., 2013; Published by CSS Bookshops Limited, Lagos Nigeria.